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首页> 外文期刊>Rivista Italiana di Paleontologia e Stratigrafia >SERPUKHOVIAN CONODONT SEQUENCE AND THE VISEAN- SERPUKHOVIAN BOUNDARY IN SOUTH CHINA
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SERPUKHOVIAN CONODONT SEQUENCE AND THE VISEAN- SERPUKHOVIAN BOUNDARY IN SOUTH CHINA

机译:中国南部的瑟鲁普霍夫牙形石序列和维塞南-瑟鲁普霍夫边界

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摘要

This paper describes in detail the conodont sequence of Upper Visean (equivalent to Tatangian of China), Serpukhovian (equivalent to Duwuan of China) and the base of Bashkirian (equivalent to Luosuan of China) in South China. The following conodont zones can be recognized in descending order: Declinognathodus noduliferus, Gnathodus bilineatus bollandensis, Lochriea cruciformis, L. ziegleri and L. nodosa zones. The first occurrences of Lochriea ziegleri and D. noduliferus (or D. lateralis) are considered as the bases of Serpukhovian and Bashkirian, respectively. The correlation of the conodont sequence from Upper Visean to the base of Bashkirian between South China and the Moscow Basin, South Urals, Great Britain, Ireland and North America is discussed.
机译:本文详细介绍了华南地区上Visean(相当于中国的Tatangian),Serpukhovian(相当于中国的Duwuan)和Bashkirian(相当于中国的Luouan)的牙形石序列。可以按降序识别以下牙形石区域:Declinognathodus noduliferus,Gnathodus bilineatus bollandensis,Lochriea cruciformis,L. ziegleri和L. nodosa地区。 Lochriea ziegleri和D. noduliferus(或D.lateralis)的首次出现分别被认为是Serpukhovian和Bashkirian的基地。讨论了华南与莫斯科盆地,南乌拉尔,大不列颠,爱尔兰和北美之间上Visean与Bashkirian基部的牙形石序列的相关性。

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